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Effect of climatic factors on the dynamics of radial increments of Norway spruce, European beech and sessile oak

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Figure

Table 1.  Stands characteristic of research plots
Fig. 1. Precipitation totals and average temperatures at Sliač climatic station
Fig. 3. Proportions of spruce trees with significant effects of precipitation (left) and temperature (right) on increment on all plots
Fig. 4. Proportions of beech trees with significant effects of precipitation (left) and temperature (right) on increment on all plots
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